嫦娥六号着陆区撞击坑的生成量

Fanglu Luo, Zhiyong Xiao, Yichen Wang, Yizhen Ma, Rui Xu, Senmiao Wang, Minggang Xie, Yunhua Wu, Qingyun Deng and Pei Ma
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引用次数: 0

摘要

嫦娥六号任务完成了首次月球远侧样品的返回。早先的陨石坑群测量估计着陆母岩的模型年龄为厄拉托什纪到晚尹布里亚纪,而早先返回的样本对这两个年龄段的代表性都不足。根据样本的同位素年龄为月球撞击通量建立一个新的校准点是很有希望的,但着陆红土的代表性陨石坑密度(即 D ≥ 1 km 的陨石坑的空间密度;N(1))对这一目的同样重要,它缺乏良好的约束条件。在排除了背景二次曲线、陨石坑平衡和观测不确定性对陨石坑统计的影响之后,这项工作从着陆母熊的多个子区域提取了不同直径范围(∼200 m-2 km)的生成群。对生产群的交叉验证验证了在草图区域直接测量直径≥1 km的陨石坑得出的N(1)是可靠的,西部和东部母雷的N(1)分别为(2.01 ± 0.90) × 10-3和(6.05 ± 2.71) × 10-3 km2。
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The Production Population of Impact Craters in the Chang’E-6 Landing Mare
The Chang’E-6 mission accomplished the first sample return from the lunar farside. Earlier crater population measurements estimated the model age of the landing mare to range from the Eratosthenian to Late Imbrian, both of which are underrepresented by earlier returned samples. Establishing a new calibration point for lunar impact flux based on isotopic ages of the samples is promising, but the representative crater density for the landing mare (i.e., spatial density of craters with D ≥ 1 km; N(1)) is equally important for this purpose, which lacks good constraints. After excluding the effects of background secondaries, crater equilibrium, and observational uncertainties on crater statistics, this work extracts production populations in different diameter ranges (∼200 m–2 km) from multiple subareas of the landing mare. Cross-validation of the production populations verifies that N(1) derived from direct measurements of craters with D ≥ 1 km in sketched areas are reliable, which is (2.01 ± 0.90) × 10−3 and (6.05 ± 2.71) × 10−3 km2 for the western and eastern mare, respectively.
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